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In situ characterization of grain‐scale fluvial morphology using Terrestrial Laser Scanning

Open access
Hodge, Rebecca, Brasington, James, Richards, Keith·2009·Earth Surface Processes and Landforms

Abstract

The grain‐scale morphology of fluvial sediments is an important control on the character and dynamics of river systems; however current understanding of its role is limited by the difficulties of robustly quantifying field surface morphology. Terrestrial Laser Scanning (TLS) offers a new methodology for the rapid acquisition of high‐resolution and high‐precision surface elevation data from in situ sediments. To date, most environmental and fluvial applications of TLS have focused on large‐scale systems, capturing macroscale morphologies. Application of this new technology at scales necessary to characterize the complexity of grain‐scale fluvial sediments therefore requires a robust assessment of the quality and sources of errors in close‐range TLS data. This paper describes both laboratory and field experiments designed to evaluate close‐range TLS for sedimentological applications and to develop protocols for data acquisition. In the former, controlled experiments comprising high‐resolution scans of white, grey and black planes and a sphere were used to quantify the magnitude and source of three‐dimensional (3D) point errors resulting from a combination of surface geometry, reflectivity effects and inherent instrument precision. Subsequently, a methodology for the collection and processing of grain‐scale TLS data is described through an application to a coarse grained gravel system, the River Feshie (D50 32 to 63 mm). This stepwise strategy incorporates averaging repeat scans and filtering scan artefact and non‐surface points using local 3D search algorithms. The sensitivity of the results to the filter parameter values are assessed by careful internal validation of Digital Terrain Models (DTMs) created from the resulting point cloud data. The transferability of this methodology is assessed through application to a second river, Bury Green Brook, dominated by finer gravel (D50 18 to 33 mm). The factor limiting the resolution of DTMs created from this second dataset was found to be the relative sizes of the laser footprint and smallest grains. Copyright © 2009 John Wiley & Sons, Ltd.

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Crossref · 10.1002/esp.1780

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Cites

  • Reconstruction and representation of 3D objects with radial basis functions

    Carr, J. C., Beatson, R. K., Cherrie, J. B., Mitchell, T. J., Fright, W. R., McCallum, B. C., & Evans, T. R. (2001) · Proceedings of the 28th annual conference on Computer graphics and interactive techniques · doi:10.1145/383259.383266 · Cited by 1,852 · cited 1×

    “It is therefore suggested that future work is needed in the development of 3D algorithms for surface interpolation (potentially such as the radial basis function approach, Carr et al., 2001) and for the measurement of properties from such 3D surfaces.”
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Metadata

Authors
Hodge, R., Brasington, J., & Richards, K.
Venue
Earth Surface Processes and Landforms
Publisher
Wiley
Published
2009-04-14
Volume
34
Issue
7
Pages
954-968
ISSN
  • 0197-9337 (ISSN-L)
  • 1096-9837
OpenAlex
W2035906824
Cited by
185
References
1
FWCI
16.20
Type
journal article
Language
en
Open access
green

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